Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Regions
South Coast.
Stiff wind slabs in the alpine are decreasing in sensitivity to human triggers. Lingering reactive wind slabs are most likely in wind-loaded areas: below ridgelines, under cornices, and around steep, unsupported features.
Confidence
High -
Weather Forecast
FRIDAY NIGHT: Mostly cloudy, isolated flurries. Treeline temperatures near -10C. Ridgetop winds strong to extreme from the northeast.SATURDAY: Mix of sun and cloud. Treeline temperatures near -6C. Ridgetop winds strong decreasing to moderate from the northeast.SUNDAY: Sunny with clouds, chance of flurries overnight. Treeline temperatures near -7C. Ridgetop winds light from the east.MONDAY: Mix of sun and cloud. Treeline temperatures near -8C. Ridgetop winds moderate from the northeast.
Avalanche Summary
Recent winds developed slabs on steep, alpine features. On Monday MIN from Mt. Anif showed substantial wind loading and a reactive wind slab problem at treeline and alpine elevations (see report here). Wind slabs were most reactive early in the week, however winds continue to redistribute loose, dry snow.
Snowpack Summary
In the alpine, 40-60 cm of wind affected snow sits above a crust or old wind pressed snow surfaces. This tapers significantly below treeline and new surface hoar is forming. Strong outflow winds have redistributed and formed isolated wind slabs at most elevations. Loose dry sluffing within the recent snow can be found in steeper terrain features. The mid-pack is well-settled and strong.
Problems
Wind Slabs
Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.